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En Eubée (Grèce), J. Deprat attribue les calcaires des monts Pyxaria et Kandili au Crétacé inférieur sous prétexte qu’ils contiennent des fossiles caractéristiques du Barrémien et de l’Albien et qu’ils passent progressivement à des calcaires cénomaniens. Or, ces calcaires ont été datés depuis du Trias et du Jurassique et le Cénomanien est partout transgressif. D’une façon générale, exception faite...
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